Unconsolidated sediments are defined here as
being composed of predominantly sand-size or smaller (<2 mm mean diameter)
grains. It may be hard, without actually moving material around on the
seafloor, to distinguish between rubble or boulders or solid rock. Rubble and
boulders may also be covered by benthic algae or other colonizing organisms,
further complicating their differentiation. Accordingly, they are included here
within the "hardbottom" category. Sand-sized or smaller sediments, on the
other hand, are relatively mobile
and tend to preclude the settlement and growth of many benthic
colonizing organisms, making them easier to distinguish from rubble, boulders,
and solid rock. If it is not possible to distinguish whether the material is
composed of sand or mud sized grains, substrate is recorded as
"unconsolidated."